Variability in Global-Scale Circulations and Their Impacts on Atlantic Tropical Cyclone Activity

In this study, intraseasonal variations in Southern Hemisphere mid-latitude large-scale circulations are examined with respect to environmental factors over the tropical North Atlantic that may be favorable or unfavorable for tropical cyclone formation. Favorable impacts on tropical Atlantic circula...

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Bibliographic Details
Main Author: Rosencrans, Matthew J.
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA DEPT OF METEOROLOGY
Format: Text
Language:English
Published: 2006
Subjects:
Meteorology
*ATLANTIC OCEAN
*CIRCULATION
*TROPICAL CYCLONES
ANOMALIES
THESES
ORTHOGONALITY
DISPERSIONS
ROSSBY WAVES
MONSOONS
CONVECTION(ATMOSPHERIC)
OSCILLATION
VORTICES
WIND SHEAR
INTRASEASONAL VARIABILITY
SOUTHERN HEMISPHERE MID-LATITUDES
TROPICAL NORTH ATLANTIC
ANTARCTIC OSCILLATION
Antarctic
Pacific
Antarc*
North Atlantic
Online Access:http://www.dtic.mil/docs/citations/ADA457680
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA457680
Description
Summary:In this study, intraseasonal variations in Southern Hemisphere mid-latitude large-scale circulations are examined with respect to environmental factors over the tropical North Atlantic that may be favorable or unfavorable for tropical cyclone formation. Favorable impacts on tropical Atlantic circulation characteristics are defined by an increase in low-level relative vorticity, a decrease in westerly vertical wind shear, and increased convection in the West African monsoon (WAM). The second and third modes of an empirical orthogonal function (EOF) analysis of the 700-hPa height anomalies identify a distinct Rossby-wave pattern. Significant variability in the Southern Hemisphere mid-latitude circulations is related to the two EOF modes and to equatorward Rossby-wave dispersion. Formation of a large cyclonic anomaly over the southeast Pacific, west of Chile, is related to equatorward propagation of a Rossby-like wave across South America, toward the equatorial Atlantic. The cyclonic anomaly precedes an increase in WAM convection by an average of two days, which then precedes westerly wind anomalies over the equatorial North Atlantic by several days. Tropical cyclone formation is found to be enhanced when the increased equatorial westerly anomalies coincide with reduced vertical wind shear, which is related to Northern Hemisphere midlatitude circulations. The original document contains color images.

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